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Poland Travel & Tourism Guide
Geology of Poland


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Granite crags of the High Tatras

The geological structure of Poland has been shaped by the continental collision of Europe and Africa over the past 60 million years, on the one hand, and the Quaternary glaciations of northern Europe, on the other. Both processes shaped the Sudetes and the Carpathian Mountains. The moraine landscape of northern Poland contains soils made up mostly of sand or loam, while the ice age river valleys of the south often contain loess. The Cracow-Częstochowa Upland, the Pieniny, and the Western Tatras consist of limestone, while the High Tatras, the Beskids, and the Karkonosze are made up mainly of granite and basalts. The Polish Jura Chain is one of the oldest mountain ranges on earth.

Source: Wikipedia Encyclopedia

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History of Poland: Poland Prehistory, Piast Dynasty of Poland, Jagiellon Dynasty of Poland, Polish-Lithuanian Commonwealth, Partitions of Poland, Reconstitution of Poland, World War II of Poland, Postwar Communist Poland, Democratic Poland, Demographics of Poland, Geography of Poland, Rivers in Poland, Geology of Poland, Mountains & Topography, Lakes in Poland, The Coast of Poland, The Desert of Poland, Land Use of Poland, Flora & Fauna of Poland, Climate of Poland, Government of Poland, Administrative Divisions, Economy of Poland, Religion in Poland, Education in Poland, Telecommunication and IT,
Culture of Poland: Famous People of Poland, Cuisine in Poland, Architecture in Poland, Sports in Poland,



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